Gföhl Unit

E884890

The Gföhl Unit is a high-grade metamorphic rock complex within the Bohemian Massif, notable for its granulites and migmatites formed under extreme pressure and temperature conditions.

All labels observed (1)

Label Occurrences
Gföhl Unit canonical 1

How this entity was disambiguated

Statements (30)

Predicate Object
instanceOf geological unit ⓘ
metamorphic rock complex ⓘ
characterizedBy extreme pressure conditions ⓘ
extreme temperature conditions ⓘ
contains felsic granulites ⓘ
mafic granulites ⓘ
migmatitic gneiss ⓘ
orthogneiss ⓘ
paragneiss ⓘ
formedDuring Paleozoic ⓘ
linked to: Paleozoic Era

Variscan metamorphic event ⓘ
linked to: Variscan orogeny
hasLithology granulite ⓘ
migmatite ⓘ
hasMetamorphicFacies amphibolite facies ⓘ
granulite facies ⓘ
hasPetrologicalFeature high-pressure mineral assemblages ⓘ
migmatization ⓘ
partial melting ⓘ
locatedIn Austria ⓘ
Central Europe ⓘ
Czech Republic ⓘ
metamorphicGrade high-grade metamorphism ⓘ
overlies Moldanubian basement ⓘ
linked to: Moldanubian Zone

Monotonous Unit ⓘ
partOf Bohemian Massif ⓘ
Moldanubian Zone ⓘ
researchedFor Variscan tectonometamorphic evolution ⓘ
crustal thickening processes ⓘ
exhumation of deep crustal rocks ⓘ
tectonicSetting Variscan orogen ⓘ
linked to: Variscan orogeny

How these facts were elicited

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.

Moldanubian Zone → contains → Gföhl Unit ⓘ